The new result focuses on ice loss due to a major retreat of
an outlet glacier connected to a long “river” of ice—known as an ice stream—that drains ice from the interior of the ice sheet. The
Zachariae ice stream retreated about 20 kilometers (12.4 miles) over the last decade, the
researchers concluded. For comparison, one of the fastest moving glaciers, the
Jakobshavn ice stream in southwest Greenland, has retreated 35 kilometers (21.7
miles) over the last 150 years.

Ice streams drain ice basins, the same way the Amazon River drains the very large Amazon water basin. Zachariae is the largest ice stream in
a drainage basin that covers 16 percent of the Greenland ice sheet—an area
twice as large as the one drained by Jakobshavn.

This paper represents the latest finding from
GNET, the GPS network in Greenland that measures ice loss by weighing the ice sheet as it
presses down on the bedrock.

“Northeast Greenland is very cold. It used to be considered
the last stable part of the Greenland ice sheet,” explained GNET lead
investigator
Michael Bevis of The Ohio State University. “This study shows that
ice loss in the northeast is now accelerating. So, now it seems that all of the
margins of the Greenland ice sheet are unstable.”

Historically, Zachariae drained slowly, since it had to
fight its way through a bay choked with floating ice debris. Now that the ice
is retreating, the ice barrier in the bay is reduced, allowing the glacier to
speed up—and draw down the ice mass from the entire basin.

“This suggests a possible positive feedback mechanism
whereby retreat of the outlet glacier, in part due to warming of the air and in
part due to glacier dynamics, leads to increased dynamic loss of ice upstream.
This suggests that Greenland's contribution to global sea level rise may be
even higher in the future,” said Bevis, who is also the Ohio Eminent Scholar in
Geodynamics and professor of
earth sciences at Ohio State.

“The fact that the mass loss of the Greenland Ice Sheet has
generally increased over the last decades is well known,” Khan said, “but the
increasing contribution from the northeastern part of the ice sheet is new and
very surprising.”

GNET, short for “Greenland GPS Network,” uses the earth’s
natural elasticity to measure the mass of the ice sheet. As previous Ohio State
studies revealed, ice weighs down bedrock, and when the ice melts away,
the bedrock rises measurably in response. More than 50 GNET stations along
Greenland’s coast weigh the ice sheet like a giant bathroom scale.

They found that the northeast Greenland ice sheet lost about
10 billion tons of ice per year from April 2003 to April 2012.

According to previous measurements and aerial photographs,
the northeast Greenland ice sheet margin appeared to be stable for 25 years—until
2003. Around that time, a string of especially warm summers triggered increased
melting and calving events, which have continued to the present day.

A large calving event at the Zachariae glacier made the news
in May 2013, and Khan and his team witnessed and filmed a similar event in
July.

Increased ice flow in this region is particularly troubling,
Khan said, because the northeast ice stream stretches more than 600 kilometers
(about 373 miles) into the center of the ice sheet, where it connects with the
heart of Greenland’s ice reservoir.

“This implies that changes at the margin can affect the mass
balance deep in the center of the ice sheet. Furthermore, due to the huge size
of the northeast Greenland ice stream, it has the potential of significantly
changing the total mass balance of the ice sheet in the near future,” he added.

Bevis agreed: “The fact that this ice loss is associated
with a major ice stream that channels ice from deep in the interior of the ice
sheet does add some additional concern about what might happen.”

The Greenland ice sheet is thought to be one of the largest
contributors to global sea level rise over the past 20 years, accounting for
0.5 millimeters of the current total of 3.2 millimeters of sea level rise per
year.